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Relevant bibliographies by topics / Ottnangian/Karpatian

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Journal articles

Academic literature on the topic 'Ottnangian/Karpatian'

Author: Grafiati

Published: 3 June 2025

Last updated: 31 July 2025

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Journal articles on the topic "Ottnangian/Karpatian"

1

Hajek-Tadesse, Valentina, Mirko Belak, Jasenka Sremac, Davor Vrsaljko, and Lara Wacha. "Early Miocene ostracods from the Sadovi section (Mt Požeška gora, Croatia)." Geologica Carpathica 60, no. 3 (2009): 251–62. http://dx.doi.org/10.2478/v10096-009-0017-0.

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Early Miocene ostracods from the Sadovi section (Mt Požeška gora, Croatia)The study of the Early Miocene (Late Ottnangian/Early Karpatian) ostracod fauna from the Sadovi section (Mt Požeška gora, Croatia) led to several results concerning Neogene paleobiogeography and paleoecology. Brackish deposits of Late Ottnangian and Early Karpatian age have been recognized for the first time in the North Croatian Basin. These deposits indicate the first marine ingression into the Early Miocene lake in this area. Twenty-nine ostracod species were determined, including the new taxaFabaeformiscandona slavon

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2

Palzer-Khomenko, Markus, Michael Wagreich, Mădălina-Elena Kallanxhi, et al. "Facies, palaeogeography and stratigraphy of the lower Miocene Traisen Formation and Wildendürnbach Formation (former “Oncophora Beds”) in the Molasse Zone of Lower Austria." Austrian Journal of Earth Sciences 111, no. 1 (2018): 75–91. http://dx.doi.org/10.17738/ajes.2018.0006.

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Abstract A detailed study of OMV wells throughout the Lower Austrian Molasse Basin demonstrates the existence of a distinct and synchronous upper Ottnangian (lower Miocene) stratigraphic signal, the Calcite Minimum Interval (CMI). It corresponds to the depositional phase of the Rzehakia Lake System. This signal is interpreted to be of chronostratigraphic importance as an expression of palaeoclimate and related sea-level change. It is represented by the brackish Traisen Formation, which crops out south of the Danube. The Traisen Formation correlates with sands and shales in OMV wells to the nor

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3

Gašparič, Rok, Dale Tshudy, Tin-Yam Chan, and Stjepan Ćorić. "A new deepwater lobster, Metanephrops serendipitus sp. nov. (Crustacea, Decapoda, Nephropidae), from lower Miocene of Meljski hrib (Maribor, Slovenia)." Boletín de la Sociedad Geológica Mexicana 73, no. 3 (2021): A240521. http://dx.doi.org/10.18268/bsgm2021v73n3a240521.

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A new species of nephropid lobster, Metanephrops serendipitus sp. nov., is described from the lower Miocene (Ottnangian/Karpatian) in beds of Central Paratethys. Metanephrops serendipitus sp. nov. represents the first fossil representative of the genus from the northern hemisphere and thus extends its known palaeobiogeographical distribution. Additionally, the palaeoecology of the new species is discussed. Similar to extant species of Metanephrops, the fossil nephropid inhabited a fine-grained deep-sea environment, associated with frequent brittle stars.

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4

Palzer-Khomenko, Markus, Michael Wagreich, Wolfgang Knierzinger, et al. "A calcite crisis unravelling Early Miocene (Ottnangian) stratigraphy in the North Alpine–Carpathian Foreland Basin: a litho- and chemostratigraphic marker for the Rzehakia Lake System." Geologica Carpathica 69, no. 4 (2018): 315–34. http://dx.doi.org/10.1515/geoca-2018-0019.

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Abstract Within the Lower Austrian part of the North Alpine Foreland Basin (NAFB), up to 1000 m of sediments were deposited throughout the Ottnangian (Early Miocene, Burdigalian). According to homogeneous compositions and sparse biostratigraphic resolution, a consistent stratigraphic concept from the basin margins into the foreland depocenter was still lacking. New investigations on several deep drill cores throughout the basin provide comprehensive sedimentological, mineralogical, chemical and micropaleontological data. A calcite poor, fossil- and pyrite-free, smectite-rich, up to 800 m thick

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5

Hyžný, Matúš, Mathias Harzhauser, and Wolfgang Danninger. "Decapod Crustacea of the Central Paratethyan Ottnangian Stage (middle Burdigalian): implications for systematics and biogeography." Geologica Carpathica 66, no. 3 (2015): 217–33. http://dx.doi.org/10.1515/geoca-2015-0021.

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AbstractDecapod crustaceans from the Ottnangian (middle Burdigalian, Lower Miocene) of the Western and Central Paratethys remain poorly known. In this study, we review and re-describe mud shrimps (Jaxea kuemeli), ghost shrimps (Gourretiasp.,Calliax michelottii) and brachyuran crabs of the families Leucosiidae, Polybiidae and Portunidae. A dorsal carapace of the genusCalliaxis reported for the first time in the fossil record. Re-examination of the type material ofRandallia strouhali(Leucosiidae) andGeryon ottnangensis(Geryonidae) resulted in a transfer of these species intoPalaeomyra(Leucosiida

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6

Šarinová, Katarína, Samuel Rybár, Fred Jourdan, et al. "40Ar/39Ar geochronology of Burdigalian paleobotanical localities in the central Paratethys (south Slovakia)." Geologica Acta 19 (May 21, 2021): 1–19. http://dx.doi.org/10.1344/geologicaacta2021.19.5.

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The Lipovany and Mučín paleobotanical localities contain important floral associations within the tuff horizons, which were used for determination of subtropical to tropical climatic conditions during the Early Miocene. Based on the combination of results from plagioclase and biotite 40Ar/39Ar dating, the age of the tuff deposition is around 17.3Ma. For the Lipovany locality, single-grain 40Ar/39Ar convergent ages of 17.49±0.54Ma and 17.28±0.06Ma, for plagioclase and biotite were obtained, respectively. The Mučín locality only provide an imprecise convergent age of 16.5±1.4Ma due to the small

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7

Harzhauser, Mathias, Matthias Kranner, Oleg Mandic, Philipp Strauss, Wolfgang Siedl, and Werner E. Piller. "Miocene lithostratigraphy of the northern and central Vienna Basin (Austria)." Austrian Journal of Earth Sciences 113, no. 1-2 (2020): 169–99. http://dx.doi.org/10.17738/ajes.2020.0011.

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Abstract For the first time, a concise lithostratigraphic scheme for the lower and middle Miocene (Ottnangian – Badenian) of the northern and central Vienna Basin is proposed, which is based on the integration of core-material, well-log data and seismic information from OMV. For all formations and members type sections are proposed, geographic distribution and thickness are provided, typical depositional environments and fossils are described and age constraints are discussed. This time frame allows for a more reliable calculation of sedimentation rates. This in turn might be important for the

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8

Meszar, Maria, Susanne Gier, Markus Palzer-Khomenko, Wolfgang Knierzinger, and Michael Wagreich. "Clay mineralogy of Miocene mudstones from the Lower Austrian Molasse Basin." Austrian Journal of Earth Sciences 113, no. 1 (2020): 125–38. http://dx.doi.org/10.17738/ajes.2020.0008.

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Abstract Recent studies established the lithological and chemical sediment evolution in the Lower Austrian Molasse Basin (LAMB), a part of the North Alpine foreland basin, during the Early Miocene. In this study, we aim to integrate the clay mineralogy of seven wells across the LAMB with a newly proposed lithostratigraphy, and to infer implications for provenance, palaeo-geography and palaeoclimate. The results of our qualitative and quantitative evaluation of the clay-sized fraction with x-ray diffractometry largely support the stratigraphic model. The early stage of foreland basin formation

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9

Hyžný, Matúš. "Diversity and distribution patterns of the Oligocene and Miocene decapod crustaceans (Crustacea: Malacostraca) of the Western and Central Paratethys." Geologica Carpathica 67, no. 5 (2016): 471–94. http://dx.doi.org/10.1515/geoca-2016-0030.

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AbstractDecapod associations have been significant components of marine habitats throughout the Cenozoic when the major diversification of the group occurred. In this respect, the circum-Mediterranean area is of particular interest due to its complex palaeogeographic history. During the Oligo-Miocene, it was divided in two major areas, Mediterranean and Paratethys. Decapod crustaceans from the Paratethys Sea have been reported in the literature since the 19thcentury, but only recent research advances allow evaluation of the diversity and distribution patterns of the group. Altogether 176 speci

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10

Prokop, Jakub, Günther Fleck, and André Nel. "New dragonflies from the Lower Miocene (Ottnangian/Karpatian) of the Cypris Shale in western Bohemia (Odonata: Libellulidae)." Neues Jahrbuch für Geologie und Paläontologie - Monatshefte 2003, no. 9 (2003): 561–76. http://dx.doi.org/10.1127/njgpm/2003/2003/561.

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